🤓 Based on our data, we think this question is relevant for Professor Nash's class at PURDUE.
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Just as the depletion of stratospheric ozone threatens life on Earth today, its accumulation was one of the crucial processes that allowed life to develop in prehistoric times:
3O2 (g) → 2O3 (g)
At a given instant, the reaction rate in terms of [O2] is 2.17 x 10-5 mol/L•s. What is it in terms of [O3]? Enter your answer in scientific notation.